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\section{Spatial discretization of the dynamical equations} |
\section{Spatial discretization of the dynamical equations} |
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Spatial discretization is carried out using the finite volume |
Spatial discretization is carried out using the finite volume |
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method. This amounts to a grid-point method (namely second-order |
method. This amounts to a grid-point method (namely second-order |
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\section{Continuity and horizontal pressure gradient terms} |
\section{Continuity and horizontal pressure gradient terms} |
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The core algorithm is based on the ``C grid'' discretization of the |
The core algorithm is based on the ``C grid'' discretization of the |
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continuity equation which can be summarized as: |
continuity equation which can be summarized as: |
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evaporation and only enters the top-level of the {\em ocean} model. |
evaporation and only enters the top-level of the {\em ocean} model. |
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\section{Hydrostatic balance} |
\section{Hydrostatic balance} |
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The vertical momentum equation has the hydrostatic or |
The vertical momentum equation has the hydrostatic or |
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quasi-hydrostatic balance on the right hand side. This discretization |
quasi-hydrostatic balance on the right hand side. This discretization |